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・ Rhodognaphalon mossambicense
・ Rhodogorgonales
・ Rhodographa
・ Rhodogune
・ Rhodogune of Parthia
・ Rhodohypoxis
・ Rhodoleia
・ Rhodoleia championii
・ Rhodoleptus
・ Rhodoleptus comis
・ Rhodoleptus femoratus
・ Rhodoleptus nigripennis
・ Rhodoleptus umbrosus
・ Rhodolfo
・ Rhodolite
Rhodolith
・ Rhodomelaceae
・ Rhodomena
・ Rhodometra
・ Rhodometra sacraria
・ Rhodometrini
・ Rhodomicrobium
・ Rhodomicrobium udaipurense
・ Rhodomicrobium vannielii
・ Rhodomonas
・ Rhodomyrtus
・ Rhodomyrtus macrocarpa
・ Rhodomyrtus psidioides
・ Rhodomyrtus tomentosa
・ Rhodon


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Rhodolith : ウィキペディア英語版
Rhodolith

Rhodoliths are colorful, unattached, branching, crustose benthic marine red algae that resemble coral. Rhodolith beds create biogenic habitat for diverse benthic communities. Common rhodolith species include ''Lithophyllum margaritae'', ''Lithothamnion muellerii'', and ''Neogoniolithon trichotomum''.
The rhodolithic growth habit has been attained by a number of unrelated coralline red algae, organisms that deposit calcium carbonate within their cell walls to form hard structures that closely resemble beds of coral. Unlike coral, rhodoliths do not attach themselves to the rocky seabed. Rather, they roll like tumbleweeds along the seafloor until they become too large in size to be mobilised by the prevailing wave and current regime. They may then become incorporated into a semi-continuous algal mat. While corals are animals that filter plankton and other organisms from the water for food, rhodoliths produce energy through photosynthesis (i.e. they can only grow and survive in the shallow photic zone of the ocean). Scientists believe rhodoliths have been present in the world's oceans since at least the Eocene epoch, some 55 million years ago.〔(''Science Daily'', September 23, 2004 )〕
== Habitat ==
Rhodolith beds have been found throughout the world's oceans, including in the Arctic near Greenland, off eastern Australia〔Harris, P.T., Tsuji, Y., Marshall, J.F., Davies, P.J., Honda, N., Matsuda, H., 1996. Sand and rhodolith-gravel entrainment on the mid- to outer-shelf under a western boundary current: Fraser Island continental shelf, eastern Australia. Marine Geology 129, 313-330.〕 and in waters off British Columbia, Canada. Globally, rhodoliths fill an important niche in the marine ecosystem, serving as a transition habitat between rocky areas and barren, sandy areas. Rhodoliths provide a stable and three-dimensional habitat onto which a wide variety of species can attach, including other algae, commercial species such as clams and scallops, and true corals.〔 Living rhodolith beds are widely distributed throughout the Gulf of California, Mexico.〔(source:Diana Steller, Moss Landing Marine Laboratories )〕 Rhodoliths are resilient to a variety of environmental disturbances, but can be severely impacted by harvesting of commercial species.
In shallow water and high-energy environments, rhodoliths are typically mounded, thick or unbranched; branching is also rarer in deeper water, and most profuse in tropical, mid-depth waters.〔

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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